Crash Course Ecology

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Crash Course Ecology Notes Created By Jack Lance The History of Life on Earth About 4 billion years ago, when the Earth’s first oceans formed, life happened via the bonding and reactions of molecules found in the water. We don’t know how it happened , but it did. First life was likely a grouping of chemicals surrounding a membrane , because as we know, phospholipids (being hydrophobic) spontaneously form bilayers when in water. Over time, these likely transformed into amino acids, and eventually RNA . These collections of chemicals trapped in membranes, called protobionts , most likely began to grow, split and replicate until some copying error gave way to DNA nucleotides, which is a much more stable repository for genetic material than RNA because it is double stranded, not single stranded (RNA). First living things were Prokaryotes , singlecelled organisms with no nuclei, that were probably very similar to the archaea we find living today in hydrothermal vents, sulfur hot springs, etc.. (Extremophiles ) likely showed up around 3.93.5 billion years ago during the Archaean Eon. The first of 3 eons in Earth’s history. The Archaean The Proterozoic The Phanerozoic These are broken up into Eras, Periods and Epochs From 3.53.1 billion years ago, prokaryotes were all alone on Earth, but then the amount of Oxygen in the atmosphere shot from 010% in a very short period of time (geologically speaking).

Transcript of Crash Course Ecology

Crash Course Ecology Notes Created By Jack Lance

The History of Life on Earth

About 4 billion years ago, when the Earth’s first oceans formed, life

happened via the bonding and reactions of molecules found in the water. We don’t know how it happened, but it did.

First life was likely a grouping of chemicals surrounding a membrane, because as we know, phospholipids (being hydrophobic) spontaneously form bilayers when in water.

Over time, these likely transformed into amino acids, and eventually RNA.

These collections of chemicals trapped in membranes, called protobionts, most likely began to grow, split and replicate until some copying error gave way to DNA nucleotides, which is a much more stable repository for genetic material than RNA because it is double stranded, not single stranded (RNA).

First living things were Prokaryotes, single­celled organisms with no nuclei, that were probably very similar to the archaea we find living today in hydrothermal vents, sulfur hot springs, etc.. (Extremophiles)

likely showed up around 3.9­3.5 billion years ago during the Archaean Eon. The first of 3 eons in Earth’s history.

The Archaean The Proterozoic The Phanerozoic

These are broken up into Eras, Periods and Epochs

From 3.5­3.1 billion years ago, prokaryotes were all alone on Earth, but then the amount of Oxygen in the atmosphere shot from 0­10% in a very short period of time (geologically speaking).

Likely produced by a new prokaryote, Cyanobacteria, which figured out how to make its own food through Photosynthesis.

This Oxygen Revolution killed off many prokaryotes that had evolved without Oxygen

About 2.1 billion years ago, a new kind of organism appeared­ Eukaryotes. These include (today) all plants and animals.

the Eukaryotes likely evolved through a process called

Endosymbiosis, in which one prokaryote parasitized another, resulting in a mutual relationship and Mitochondria.

About 1.5 billion years ago, Multicellular eukaryotic organisms begin showing up, the very first likely being algae.

Around 535 million years ago, the Eukaryotes went berserk. This is known as the Cambrian Explosion. A major

biological golden­age when the diversity of all animal life on Earth ‘exploded’.

Creatures began to use minerals to create shells, skeletal structures, claws and defensive plates.

This brought about the dawn of the Phanerozoic Eon The one we are in currently

Around 500 million years ago, during the Ordovician Period, plants, animals and fungi started colonizing the land (likely to escape predation).

During the Devonian Period, about 365 million years ago, Tetrapods (4­legged vertebrates) and Arthropods began showing up on land.

The Carboniferous Period, that extended from 359­299 million years ago, heralded a major development of plants.

The forests were so dense and widespread that they made all the fossil fuels we now use.

These forests created so much oxygen that the atmosphere was around 35% O2, rather than today’s 21%

This O2 cooled the planet, crashing the entire system. During the Permian Period, 299­251 million years ago, all

the landmasses of the world joined to form one giant continent we know as Pangea.

We begin to see Gymnosperms (the first plants with seeds), and Archosaurs.

About 252 million years ago, the Permian­Triassic Extinction took place.

96% of all marine species and 70% of terrestrial vertebrate went extinct, and is the only known mass extinction of insects (57% of all taxonomic families and 83% of all genera went extinct)

The most significant extinction event on the plant. Ever.

Dawned the age of the Dinosaurs. Not much competition allowed evolution to fill many available niches (a combination of biotic and abiotic resources that a species could use to survive).

During the Jurassic Period, about 199­145 million years ago, large herbivorous dinosaurs and smaller carnivorous dinosaurs were roaming the Earth. (There were also mammals, small, but still there)

65 million years ago, all the Dinosaurs went extinct (currently only theories suggest why), except for their surviving descendants­ the birds.

About 100 million years ago, Angiosperms, or flowering plants, appeared. Flying insects evolved with them, providing an ideal vehicle for reproduction.

Coevolution On a geological scale, that brings us up to now.

Population Ecology

Population Ecology: Groups within a species and how they interact

and live together in one geographic area. Fundamental Principles of Population Ecology include:

A population is just a group of individuals of one species who interact regularly

How often organisms interact has a lot to do with Geography. You compete with those closer to you for food, living space, reproductive privileges, etc..

Population Density, or how many of a population are in a specific area that might come into contact with each other.

Geographic Arrangement of individuals within the population. This is also known as Dispersion.

Population Growth. All kinds of factors drive this:

Fecundity (how many offspring an individual can have)

Limiting Factors, the biotic and abiotic factors that limit population growth.

Niche Requirements Mates and Mating

Categorized into: Density­Dependent(Is the population being

controlled by how many individuals are in it?)­ limit growth due to environmental stress caused by population size.

Density­Independent(Is the population being controlled by something else?)­ limit growth due to external factors like a volcanic eruption, monsoon, etc..

Carrying Capacity is the Number or individuals that a habitat can sustain with the resources available. Once Density Dependent limiting factors kick in, that’s a pretty good sign of a population reaching its carrying capacity.

Any population of anything, according to math, will grow exponentially until, for some reason, it can’t anymore.

Known as Exponential Growth. The population grows at a rate proportional to

the size of the population. Once the population reaches these limiting factors,

it will only experience Logistic Growth.

This means that the population is limited to the carrying capacity of its habitat.

Mathematical Equation for population growth:

R = (Natality ­ Mortality)/(N) R refers to Rate of growth N refers to Initial Population Size

And as for Growth over a Period:

Community Ecology: Focused on groups of different organisms living together, and figuring out how they influence each other.

Ecosystem Ecology: The study of how all living and nonliving things interact within an entire ecosystem.

Human Population Growth

Since about 1650, Human population has been undergoing the

longest period of exponential growth of any large animal in history.

In 1650, there were about 500 million people on the planet By 1850 the population had doubled to 1 billion Doubled again just 80 years later Doubled again just 45 years later Now well past 7 billion and counting

Perennial problem in nature and in our lives: Quality or Quantity? All organisms make a similar choice through how they

reproduce: R vs K Selection Theory

R vs K Selection Theory states that some organisms reproduce in a way that aims for huge, exponential growth, while others aim for a smaller, more intimate relationship with their offspring. (K reproducers are typically content only creating enough offspring to hit the Carrying Capacity of their habitat)

R­selected species produce very rapidly and do not invest time in raising offspring. R standing for the ‘maximum rate of a population’.

K­selected species only produce a few offspring within their lifetime, and invest a lot of time and energy raising them. K standing for ‘Carrying Capacity’.

Most animals aren’t very strongly K­ or R­ selected. It’s more of a spectrum: Some organisms­ usually small ones­ tend to reproduce more on the R­ side, while larger organisms tend to reproduce more on the K­ side. Most species are somewhere in the middle.

Contradiction of Humans = We tend to reproduce and raise our offspring in a K­selected manner, yet over the past 300+ years, our population curve looks suspiciously like that of an R­selected Species.

Even then, most exponential growth rates, even for R­Selected species, usually do not go on for 350 years.

We’ve been able to do this because we learned how to eliminate limiting factors that would’ve plateaued (made us reach our carrying capacity) and eventually diminished our population.

Agricultural advances Medical advances Not being so Disgusting! (Sewage) Adapting to Inhospitable Places

Ecological Footprint: Calculation of how much land and how many resources each person on the planet requires to live.

Varies geographically and determined by lifestyle.

Community Ecology

Competition: Because there is a finite amount of resources on the planet, evolution drives us to compete for them so that we can live long enough to reproduce.

Important part of how different species interact when their habitats overlap. These interactions define Ecological Communities

Interspecific Competition: When communities of the similar species compete for the same resources needed for their survival and continued population growth. i.e. weeds competing with sunflowers for the nutrients and water in soil.

Finite Resources are typically limiting factors in competition. Competitive Exclusion: When one species eliminates another

competing for the same resources. When two species are competing for the same resources, one

of them will eventually be more successful, and eliminate the other.

Not all resources are limiting. Most species, even ones that are nearly identical, are

adaptable enough to find a way to survive in the face of competition.

This is done by finding an ecological niche.­ the sum of all resources, both biotic and abiotic, that a species use in it’s environment.

Fundamental Niche: an Ideal niche in which a species can live the way it naturally wants to should there be no competition. Few species ever achieve this.

Most species, in order to avoid competitive exclusion and continue living, take up a Realized Niche­ Or, the niche in which a species lives in the presence of competitive exclusion.

Canadian Ecologist, Robert Macarthur, made a discovery that made him one of the most influential ecologists of the 20th century.

While researching at Yale in 1958, he studied 5 species of warblers that live in coniferous forests. At the time, because of the sheer amount of warblers living in the same area, many ecologists thought they occupied the same ecological niche.

Macarthur studied the birds for many seasons, dividing individual trees different warblers lived in, and observed that each species of warbler divided it’s time differently among the various parts of the tree.

The warblers had different hunting and foraging habits, and even bred at different times of the year so that their highest food requirements didn’t overlap.

This was the first recorded observation of a Realized Niche. This phenomenon is now known as Resource

Partitioning. (when similar species settle into separate niches that let them coexist)

Mutualism: When two species benefit by forming relationships through conflict­avoidance. Both provide a service, and both benefit.

Obligate Mutualism: relationship in which one species would die if the other was not there.

Commensalism: Relationship in which One species benefits, and the other is unaffected/neutral toward the relationship.

Community Ecology II: Predation

Herbivory: Predation in which an organism eats primary

producers Parasitism: Predation in which organisms derive energy from a

host, usually harming it, and sometimes killing it in the process. The need to survive causes predator and prey to adapt to develop

both weapons and defenses in a never­ending evolutionary change. Hunting and feeding adaptations for predators Detection, Capture and Handling adaptations for prey

To avoid Detection, some creatures have developed Cryptic Coloration (camouflage)

Avoiding Capture, some animals have developed speed advantages, and some find safety in numbers (like Bison), forming giant herds.

Preventing Handling can appear in many ways, such as plants growing thorns, creating sap that traps insects, chemical weapons like the tobacco plant’s nicotine, Aposematic Coloration (Warning Coloration), Mullerian Mimicry (alike coloring of similar types of poisonous species), Batesian Mimicry (The copying a poisonous creature’s appearance by non­threatening creatures)

Ecological Succession

Primary Succession: Happens during a large ecological event, such

as a volcanic eruption, glacial freeze, asteroid impact, superstorm, etc.. When organisms populate an area for the first time.

Advantage = No competition (Pioneer Species = prokaryotes/protists)

Exclusively plants, typically with wind­borne seeds like lycophytes.

Objective = to build/rebuild soils Takes a very, very long time.

Secondary Succession: Once the soils are ready, larger plants are

able to move in and repopulate. Usually the first response after a smaller disturbance like a flood or fire.

These small disturbances that stimulate secondary succession lead to development of a Microclimate (a small climate in the area of succession that slightly differs from the climate around it).

This microclimate leads to different niches, plant populations, animal populations, and can even change the ecosystem within its area.

Climax Community Model: Observation in which communities

show a tendency to morph over time, changing until it becomes a Climax Community, in which it would have a predictable assemblage of species that would remain stable until the next major disturbance.

Stochasticity: Randomness. Prevents us from ever knowing exactly what a community will look like after a disturbance. Element of unpredictable variability.

Ecosystem Stabilization: Issue because ecological communities can never really become ‘stable’, as there is always some aspect of change occurring.

We can tell that an ecosystem is in later stages of succession determinant upon its level of Biodiversity.

High Biodiversity: When there are many niches that are occupied by organisms.

Only way for there to be High BioD, is for an Ecosystem to have thousands of communities, meaning it is in the latter stages of succession.

Intermediate Disturbance Hypothesis: Theory that intermediate

disturbances (not too big, not too little), are ideal for the overall development of a community and Ecosystem.

More niches = more Biodiversity; more Biodiversity = more stability and healthier ecosystems.

Ecosystem Ecology

Defining an Ecosystem: A collection of living and nonliving things

that interact with each other in a certain way. Simultaneously­ It depends

Want to know how energy and materials come in and move through a tree with a specific community of insect protists in it? That is an ecosystem, etc...

Ecosystem can be measured via Biomass: The total weight of all living things within

the ecosystem. Productivity: How much stuff is produced and how

quickly it grows back. Retention

Where do the materials come from? (Water, Nitrogen, Phosphorus, etc..)

Energy Law of conservation of matter; same goes for

an ecosystem.

All energy (food) in an ecosystem move through it indefinitely via transference in Trophic levels.

Primary source of Energy: Solar/Photosynthesis via Primary Producers

Primary Producers are then consumed by Heterotrophs (Herbivores), aka Primary Consumers.

Primary Consumers then Eaten by Secondary Consumers and so on, until Decomposers (Detrivores) eat the dead consumers.

Efficiency of energy transference: 1/10 of energy is transferred to the

consumer.

Unfortunately, if there are toxins involved, they do

not abide by energy’s law of transference, and simply accumulate into the consuming organism.

Known as Bioaccumulation

Biogeochemical Cycles

Hydrologic Cycle: How water moves on, above, and below the surface of the Earth­ driven by energy supplied by the Sun and the Wind.

Easy to think of all the water on Earth as held in reservoirs. The Ocean The Atmosphere (clouds) The Polar Ice Caps So not only does water cycle through different places,

but also takes different forms at different places in the cycle (liquid, solid, gas).

No Beginning or End 1)Precipitation

Rain , Hail, Snow, etc.. Happens when water in the atmosphere condenses from a gas to a liquid and occasionally a solid.

(Opposite of condensation is evaporation, and when a substance converts straight from a solid to a gas, that’s sublimation, and the opposite of this is deposition)

Condensation is responsible for clouds, which happens when air containing water vapor rises and cools or is compressed to the point where it can no longer be a gas. At this point, the vapor forms droplets.

Wind moves clouds, and as water in clouds keeps condensing and getting heavier, gravity eventually takes over and pulls the condensed droplets to the ground in the form of rain, snow, hail, etc…

Gravity continues to work, pulling the water to its final resting place, typically the lowest nearby point. This is called runoff. Or the water is pulled underground.

Most water is pulled through runoff after precipitation until it eventually reaches the ocean.

The Carbon Cycle: Carbon absorbed by plants has 3 possible fates

It can be respired back into the atmosphere It can be eaten by an animal Or it can be present when the plant dies.

*So what are Nitrogen and Phosphorus used for? Animals are 3% Nitrogen and 1% Phosphorus We need Nitrogen to make Amino

Acids­>Proteins­>Bodies­>DNA & RNA DNA and RNA also require Phosphorus

ATP, and Phospholipid Bilayer Nitrogen Cycle

Nitrogen Gas (N2) makes up about 78% of the atmosphere Unfortunately, it is made up of two N atoms stuck together with

a triple bond. Very hard to break. Plants need help to assimilate the N2, and receive that help via

Nitrogen Fixation. Using Nitrogen­Fixing Bacteria. Found in soil or water, or in

symbiotic relationships with root systems in Legumes. These bacteria convert N2 into Ammonia (NH3), which then

becomes Ammonium (NH4+) when mixed with water, which can be used by plants.

They do this with a special enzyme­ Nitrogenase­ which is the only biological enzyme that can break that triple bond.

Ammonia can also be made by Decomposers like fungi when breaking down dead organic matter (proteins and DNA). Once this happens, other Nitrifying Bacteria can take this ammonia and convert it into Nitrates (NO3­)­>3 Oxygen atoms attached to a Nitrogen atom, as well as Nitrites (NO2­)

These are even easier than Ammonium for plants to assimilate

Other ways to break the bonds between the N atoms include Lightning Synthetic fixation (fertilizers)

The cycle continues (Bacteria­>Plants­>Animals­>Decomposers) UNTIL that Nitrogen finds itself in Denitrifying Bacteria, whose job it is to metabolize the Nitrogen Oxides back into Nitrogen Gas.

This process uses a special enzyme called Nitrate Reductase.

The Phosphorus Cycle

Concentrated in the Lithosphere. Rocks containing inorganic phosphates (especially

sedimentary­ originating in old ocean floors and lakes) Not many rock­eating bacteria on Earth, only Lithotrophs, so

bacteria do little to expose the phosphorus When the rocks are re­exposed (from underwater), and water

erodes them, some of the phosphates are dissolved into the water. These dissolved phosphates are immediately available to, and

assimilated by plants, which are then eaten by animals.

As in the Nitrogen cycle, decomposers then release the phosphorus back into the soil and water via decomposing dead organic organisms.

Decomposed phosphate is Immediately re­assimilated back into plants, and the cycle goes on.

Once that atom of phosphorus makes it way into some body of water, it can cycle around the organisms there for 100,000 years.

Eventually it will make its way into something that dies and falls into a hole so deep that decomposers can’t survive there and becomes sedimentation, which builds into rocks­>mountains­>erosion­>water

Humans have introduced synthetic fertilizers, containing lots and lots of nitrogen and phosphorus­ but too much of a good thing is bad. This poses intense ecological stress on ecosystems.

Human Impacts on the Environment

Human behaviour and lifestyle has already driven nearly 1,000 plant

and animal species (to date) into extinction­ most of them over the last century.

Ecosystem Services: Benefits the natural world provides us for free, typically things that we could never, ever duplicate on our own.

Thus, having Ecosystems and keeping them intact is not only important for the organisms who live in them, but also for us.

These services can be broken up into 4 categories Support Services­ create and replenish the foundation

of the Earth’s biological systems. (recycling the compounds that are necessary for life through the biogeochemical cycles, forming new soils, producing oxygen)

Provisioning Services­ providing the raw materials we need to live. (The ocean providing food, rivers give water, plant fiber for clothing and shelter, sources of fuel in the form of biomass, hydropower, fossil fuels)

Regulating Services­ Decomposers converting waste to energy, plants filtering water and air, producing oxygen and absorbing CO2, etc..

(Cultural Services) Ecosystems Just Being Awesome­ It’s nice to be surrounded by other living things, healthy ecosystems give us places to play, inspiration, grounds for education through study. Less tangible, but still important cultural services.

Ecosystems with High Biodiversity are much more resilient to and capable of handling that ‘never­ending change’, as well as being able to handle disturbances much better.

In a High Biodiversity ecosystem, if you take one species out of the mix, it’s less likely that the ecosystem will collapse.

Best way to see how we affect the environment is through how we affect biodiversity.

Unfortunately, we have already endangered most of the highest biodiversity ecosystems on the planet.

Top Five ways that humans are messing up the Environment: 1) Deforestation­ we currently cut through 8,000 hectares of

trees a day to provide land to graze cattle on, and to harvest wood

2) Desertification­ Can be a side­effect of Deforestation, in which dry, unproductive landscapes spread. Driven along by additional factors like overgrazing and over­irrigation.

Over­irrigation can cause Desertification because when we use groundwater to irrigate crops, the natural salts in that groundwater build up in the soil, eventually making it so salty that nothing can grow.

Over time, ecosystems near deserts become overtaxed, and the desert is able to spread into it.

3) Global Warming­ Increase of CO2 in the atmosphere while decrease in the area of forests and lush ecosystems that provide regulation = bad. Melting Sea Ice leads to less habitat for polar bears, seals and sea birds. More temperate animals are moving closer to the poles, and hotter, drier conditions are causing more fires.

Biggest problem with this is the time­frame of the disturbance. Changes like this have happened in the past, but took place over millennia, allowing organisms time to adapt, while these changes are taking place over our individual lifetimes.

4) Introducing Non­Native Species­ Both intentionally and unintentionally, this can lead to invasive species, rapid niche changes, and ecosystem entropy.

5) Overharvesting­ Overfishing the oceans to meet growing demand for popular fish species, over­hunting predators like wolves to protect livestock.

Pollution­ Any substance that’s in the wrong place or in the wrong concentrations in the environment.

Trash in the environment­ Pollution Chemicals in the environment (both naturally occurring and

synthetic)­ Real killers. We tend to think of pollution as chemicals made in large

chemical processing plants, and these are definitely a problem, BUT, natural compounds in wrong concentrations can do just as much damage.

One of the main ways we are altering the concentrations of natural compounds is by messing with the biogeochemical cycles.

Most obvious cycle we’re altering = Carbon Cycle Cycle keeps going on, but problem is that we’re overloading it

by digging up and burning carbon­rich coal, oil and gas. Also been tampering with Nitrogen and Phosphorus cycles,

via increasing concentrations in the environment by creating synthetic fertilizers that can spread nutrients into the water, leading to large algal blooms that ‘choke­out’ the rest of the plants and animals in the stream.

Also cause Dead Zones, in which decomposers try to decompose the algae after it has used up all of the nitrogen and phosphorus, but require Oxygen to do so, taking it out of the water, thereby killing most of the other living organisms in that area that require oxygen.

Important Natural Pollutants Cyanide (used in mining operations for ore extraction, leading

to hazardous waste that never really goes away) Mercury (Super­toxic, naturally occurring metal found in coal

among other places, and doesn’t do anything while underground in coal seams, but when that coal is burned to

make electricity­ it’s released into the air. It then falls onto the land, making its way to groundwater, and eventually into the food chain (specifically marine).

Sulfur Dioxide & Nitrogen Dioxide (Naturally sourced from volcanic eruptions and the waste of some algae and bacteria) but we release millions of tons of this stuff every year by burning fossil fuels. When they react with compounds in the atmosphere, they turn into sulfuric acid and nitric acid, returning to the surface as acid rain.

Important Synthetic Chemicals Endocrine Disruptors (EDC)­ put in pharmaceuticals,

pesticides and plastics. I.E. BPA, which is found in plastics and leach into our drinks. When they are excreted back into the environment, typically in waterways in high concentrations, animals end up absorbing them.

These alter an animal’s Endocrine (hormone) system, and have led to male fish with female reproductive tracts, or testes that make eggs.

Unknown effects on humans thus far, but research is progressing.

Conservation and Restoration Ecology

Conservation Biology

Involves measuring the biodiversity of an ecosystem and determining how to protect it.

Restoration Ecology The science of restoring broken ecosystems. For example

taking an interrupted, polluted river, and turning it into a functioning ecosystem again.

To fix something that’s broken, you have to understand what made it work to begin with. Practicality.

The glue that holds every ecosystem together is Biodiversity.

Biodiversity can mean many different things, though. It’s generally referring to species diversity.

In addition to species diversity, ecologists look at genetic diversity within a species as a whole and between populations.

Genetic Diversity is important because it allows a species to adapt to new situations and disturbances like disease and climate change.

Ecosystem Diversity is the variety of different ecosystems within an area.

A large forest, for example, can host several different ecosystems, like wetland, alpine, and aquatic.

Small Population Conservation focuses on identifying

species and populations that are miniscule, and attempts to increase their numbers and genetic diversity.

When a population is small and has low biodiversity, its very probable that it will soon die out, so when a population is suffering from inbreeding or genetic drift (a shift in it’s overall genetic makeup), this leads to even less diversity­>lower natality rates­>higher mortality rates­>even smaller population.

This is known as an Extinction Vortex So how small is too small? Ecologists figure this out by

calculating whats called the Minimum Viable Population, which is the smallest size at which a population can survive and sustain itself.

To calculate this, you need to find out a species real breeding population­ and then you figure out everything you can about that species life history:

How long they live

Who gets to breed the most How often they can create offspring, etc..

Declining Population Conservation focuses on populations whose numbers are in decline no matter how large the original population was.

First one must determine whether the population is actually declining

Then you have to determine how large the population historically was and what its requirements were

Finally, you must determine what is causing the decline and figure out how to address it

Of course, we can’t really bring an ecosystem exactly back to the way it used to be, but through these sciences, we can get rid of the problems they are facing and recreate some of the elements that the ecosystem needs to function properly.

Structural Restoration is the removal and cleanup of whatever human impact was causing the problem, and the rebuilding of the historical natural structure.

Bioremediation recruits organisms temporarily to help remove toxins, like bacteria that eat wastes or plants that leach out metals from tainted soils.

Biological Augmentation is a somewhat more ‘invasive’ method of restoration in which rather than removing harmful substances, organisms are added to the ecosystem to restore materials that are gone.

i.e. plants that help fix nitrogen like beans, acacia trees and lupine are often used to replenish nitrogen in soils that have been damaged by things like mining and over­farming.

Problems can lead to introduction of an invasive species

i.e. 1930’s Australia introduction of cane toads to control beetles. Not only are they toxic, but they’re everywhere now, and poison native species like dingos that try to eat them.

Thus, its just easier to Protect Ecosystems rather than trying to fix them.

Sources and Citations

1. Crash Course Ecology

a. Crash Course Ecology. Hank Green. Crash Course Ecology Series, 2012­2013. Web. 10 Feb. 2015. <https://www.youtube.com/watch?v=sjE­Pkjp3u4&index=1&list=PL8dPuuaLjXtNdTKZkV_GiIYXpV9w4WxbX>